The Deep Hydrocarbon Cycle: From Subduction to Mantle Upwelling

Autor:	A. Yu. Serovaiskii, A. N. Dmitrievsky, Vladimir G. Kutcherov, Kirill S. Ivanov
Rok vydání:	2020
Předmět:	Iron hydride 010504 meteorology & atmospheric sciences Hydrogen Subduction chemistry.chemical_element Crust 010502 geochemistry & geophysics 01 natural sciences Mantle (geology) Carbide Ferrous chemistry Asthenosphere Earth and Planetary Sciences (miscellaneous) General Earth and Planetary Sciences Petrology Geology 0105 earth and related environmental sciences
Zdroj:	Doklady Earth Sciences. 492:338-341
ISSN:	1531-8354 1028-334X
DOI:	10.1134/s1028334x20050098
Popis:	Experimental results and geological observations suggesting the existence of a deep hydrocarbon cycle are presented. During immersion hydrocarbons accumulated in the Earth’s crust in the slab generally maintain stability to a depth of 50 km. With deeper immersion, the hydrocarbon fluids contact the surrounding ferrous minerals forming a mixture of iron hydride and iron carbide on the depths of 100–290 km. Iron carbide transported into the asthenosphere by convective flows can act as carbon donors and react with hydrogen donors presented in the asthenosphere and form an aqueous-hydrocarbon fluid. This fluid can migrate through deep faults into the Earth’s crust and form oil and gas deposits.
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_________::1bd2f1d0229f965fed4139ad67d5238f https://doi.org/10.1134/s1028334x20050098 Zobrazit plný text záznamu Plný text ve formátu PDF Plný text ve formátu HTML
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